Zobrazeno 1 - 10
of 156
pro vyhledávání: '"Jean-robert Petit"'
Autor:
Jean-Robert Petit, Biancamaria Narcisi
Publikováno v:
Geological Society, London, Memoirs. 55:649-664
Driven by successful achievements in recovering high-resolution ice records of climate and atmospheric composition through the Late Quaternary, new ice–tephra sequences from various sites of the East Antarctic Ice Sheet (EAIS) have been studied in
Autor:
Sergey Bulat, Jean-Robert Petit
Publikováno v:
Encyclopedia of Astrobiology ISBN: 9783642278334
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f3812e6fe5198a004a5907a9c7a10018
https://doi.org/10.1007/978-3-642-27833-4_1765-3
https://doi.org/10.1007/978-3-642-27833-4_1765-3
Publikováno v:
La Météorologie. :022
Autor:
Sergio Andò, Chiara Ileana Paleari, Barbara Delmonte, Eduardo Garzanti, Valter Maggi, Jean-Robert Petit
Publikováno v:
Geophysical Research Letters. 46:9968-9979
We analyzed the single-grain mineralogical composition of aeolian dust transported to central East Antarctica for provenance purposes. Comparison with data from the last glacial period shows for the first time disappearance of carbonates during the H
Publikováno v:
Paleontological Journal. 52:1196-1203
Comparative analysis of the Vostok ice core (Central East Antarctica; one horizon, three boreholes) and D10 ice core (shoreline nearby the French Dumont d’Urville station) has reliably revealed three phylotypes (species) of aerobic iron-oxidizing b
Autor:
Simon Schüpbach, Jiawen Ren, Chuanjin Li, Cunde Xiao, Yuefang Li, Jean-Robert Petit, Junji Cao, Paul Andrew Mayewski, Tong Zhang, Yeongcheol Han, Michael Handley, Zhiheng Du
Publikováno v:
National Science Review
Mineral dust can indirectly affect the climate by supplying bioavailable iron (Fe) to the ocean. Here, we present the records of dissolved Fe (DFe) and total Fe (TDFe) in North Greenland Eemian Ice Drilling (NEEM) ice core over the past 110 kyr BP. T
More than 2,000 analyses of beryllium‐10 (10Be) and sulphate concentrations were performed at a nominal subannual resolution on an ice core covering the last millennium as well as on shorter records from three sites in Antarctica (Dome C, South Pol
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::551f18ea30baa75f6330fc4478db9338
https://doi.org/10.5194/egusphere-egu2020-12957
https://doi.org/10.5194/egusphere-egu2020-12957
Autor:
Shohei Hattori, Vladimir Ya. Lipenkov, Elsa Gautier, Joel Savarino, Francis Albarède, Jean-Robert Petit, Nicolas Caillon, Emmanuelle Albalat
The ca. 74 ka BP ‘‘super-eruption’’ of Toba volcano in Sumatra is the largest known Quaternary eruption. It expelled an estimated of 2800 km3 of dense rock equivalent, creating a caldera of 100 x 30 km. The eruption is estimated to have been
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e36251bc75c9708c2ab79cdff570083d
https://doi.org/10.5194/egusphere-egu2020-4
https://doi.org/10.5194/egusphere-egu2020-4
Autor:
Jean-Robert Petit, Dominique Raynaud
Publikováno v:
Nature. 579:505-506
In 1980, a method was found to determine the amount of carbon dioxide in ancient air trapped in polar ice — providing direct evidence that CO2 is coupled to climate, and affects global temperatures in the past, present and future. In 1980, a method
Publikováno v:
Quaternary Science Reviews
Quaternary Science Reviews, Elsevier, 2019, 210, pp.164-174. ⟨10.1016/j.quascirev.2019.03.005⟩
Quaternary Science Reviews, 2019, 210, pp.164-174. ⟨10.1016/j.quascirev.2019.03.005⟩
Quaternary Science Reviews, Elsevier, 2019, 210, pp.164-174. ⟨10.1016/j.quascirev.2019.03.005⟩
Quaternary Science Reviews, 2019, 210, pp.164-174. ⟨10.1016/j.quascirev.2019.03.005⟩
Strong volcanic signals simultaneously recorded in polar ice sheets are commonly assigned to major low-latitude eruptions that dispersed large quantities of aerosols in the global atmosphere with the potential of inducing climate perturbations. Paren
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::32c59c93112a18d7f18e9091f5ff31f6
https://hal.archives-ouvertes.fr/hal-02350371
https://hal.archives-ouvertes.fr/hal-02350371